1, Tianmu Hot Spring Resort
Located in Shenghai Road, Zhangjiachan Town, Wendeng District, Weihai City, Shandong Province, it is a hot spring resort integrating hydrophilic rooms, green food and fresh air, and also a hot spring health and leisure resort. The resort is built on the mountain and the lake on the mountain, which constitutes the magical landscape of scarab exploring the sea. The overall architectural layout is like a flying dragon, which is consistent with the meaning of the dragon in Wendeng's hometown of Li Long.
2. Weihai Taixigu Cultural and Creative Town
Located in Wendeng District, Weihai City, Shandong Province, it is a large-scale cultural industry creative base integrating wedding custom culture, theme amusement, business leisure, hot spring recuperation, amorous feelings experience, health and holiday. B&B Wendeng Daxigu Cultural and Creative Town was selected as a five-star boutique B&B, which is a comprehensive town integrating wedding culture, theme amusement, business and leisure, amorous feelings experience, health and holiday.
3. Tianfu Mountain Uprising Memorial Hall in Wendeng District.
Located in Tianfu Mountain, Wendengying Town, Wendeng District, Weihai City, Shandong Province, the museum collects precious cultural relics, deeds, pictures and revolutionary martyrs' relics of Tianfu Mountain Uprising. The memorial hall has become an ideological education classroom for young people to remember revolutionary martyrs, relive vicissitudes of life, accept fine traditions, mourn veteran cadres and old party member, cheer up their spirits and inspire their fighting spirit.
Wendeng geographical environment
Wendeng is located in the east of the second uplift of New China and the center of Wenrong uplift. Due to long-term uplift, the Jurassic strata of Mesoproterozoic-Mesozoic were missing. The general characteristics are: simple geology, extensive distribution of magmatic rocks and undeveloped structure. The stratum is dominated by the metamorphic rock series of the second rock group of Jiaodong Group in Lower Proterozoic, and the Quaternary sediments are distributed all over the territory, including alluvial, diluvial, residual and marine sediments. The folds are simple, and the Wangtuan area in the north is an inverted anticlinorium.
It belongs to the middle section of the inversion anticlinorium from Rushan City to Huancui District of Weihai City, with an axial direction of about 45 and an axial plane inclined to the southeast. Influenced by the Kunyu Mountain rock mass, the syncline axis bends and the middle section protrudes to the northwest. Nangaocun and Houjia areas are monoclinal structures. Due to the intrusion of Weideshan, Zijinshan and other rock masses, it is not only discontinuous with the northern strata, but also uncoordinated in occurrence, forming a wide and gentle monoclinal structure that inclines and protrudes to the south. There are not many faults in China, and there are four larger ones: Muzhuhe fault, which is distributed in the north-south direction, with a length of 40 kilometers and a width of 50 ~ 100 meters.
Reference to the above contents: Baidu Encyclopedia-Tianmu Hot Spring, Baidu Encyclopedia-Daxi Valley Cultural and Creative Town